Determination of Hydraulic Properties of a Large Self-Propped Hydraulic Fracture in the Geothermal Research Borehole Horstberg Z1 in the Northwest German Basin

<div>Conceptual model for the test evaluation. White areas in the Detfurth and Solling: flow channels with infinitely high hydraulic conductivity. Black arrows illustrate fracture-linear flow in the fracture and formation linear flow in the Detfurth and Solling. T<sub>D</sub>, S<sub>D</sub>, T<sub>S</sub>, S<sub>S,</sub> T<sub>f</sub>, S<sub>f</sub>: transmissivity and storage coefficient of the Detfurth, Solling and fracture, respectively.</div>

Geofluids

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Figure 3

Figure 3: Determination of Hydraulic Properties of a Large Self-Propped Hydraulic Fracture in the Geothermal Research Borehole Horstberg Z1 in the Northwest German Basin 

Figure 3 | Determination of Hydraulic Properties of a Large Self-Propped Hydraulic Fracture in the Geothermal Research Borehole Horstberg Z1 in the Northwest German Basin 